Methanofuran-b is required for CO2 formation from formaldehyde by Methanosarcina barkeri

Abstract Extracts of Methanosarcina barkeri strain Fasaro oxidized formaldehyde to CO₂ with methyl-coenzyme M as the natural terminal electron acceptor resulting in methanogenesis. A combination of the artificial electron acceptors methylviologen and metronidazole could substitute for methyl-coenzyme M. The rate of formaldehyde oxidation was thereby increased. Taking advantage of this artificial electron acceptor system the role of cofactors in formaldehyde oxidation was investigated. Cofactor-free extract of M. barkeri did not catalyze the oxidation of formaldehyde. CO₂ formation could be restored by the addition of tetrahydromethanopterin-b (H₄MPT-b) and methanofuran-b (MFR-b) from M. barkeri . Other low molecular weight or heat-resistant compounds stimulating formaldehyde oxidation were not found. Formaldehyde oxidation seems, therefore, to proceed via H₄ MPT-b and MFR-b-derivatives already shown to be involved in methanogenesis from H₂+ CO₂.     

Sodium dependent acetate formation from CO2 in Peptostreptococcus productus (strain Marburg)

Abstract Washed cells of Peptostreptococcus productus (strain Marburg), which were incubated in the presence of CO/CO₂/N₂ (50%/ 17%/ 33%; 200 kPa) catalyzed the synthesis of acetate from carbon monoxide. The rate of acetate formation from CO was stimulated more than threefold by the addition of sodium (10 mM); potassium did not effect acetate synthesis. The degree of stimulation was dependent on the sodium concentration; the dependence followed simple Michaelis-Menten kinetics. The apparent K _m for sodium was determined to be about 2 mmol/1. Sodium also stimulated acetate synthesis from H₂ plus CO₂. In the absence of added sodium the formation of formate as an intermediate in methyl group synthesis was stimulated. It is suggested that the sodium dependent reaction(s) is one (or more) of the reactions involved in methyl group synthesis from CO₂.     

Microbial H2/CO2 acetogenesis in animal guts: nature and nutritional significance

Abstract The intestinal tract of invertebrate and vertebrate animals, including man, is an anoxic habitat wherein microbial formation of acetate from H₂+ CO₂ is often a major H₂-consuming reaction. This paper will discuss the magnitude and microbiology of H₂/CO₂ acetogenesis in animal guts, its impact on host animal nutrition, competition for H₂ between anaerobic microbes, and the global significance of intestinal H₂/CO₂ acetogenesis.     

K+ATP channel opening prevents succinate-dependent H2O2 generation by plant mitochondria

The role of a recently identified K⁺_ATP channel in preventing H₂O₂ formation was examined in isolated pea stem mitochondria. The succinate-dependent H₂O₂ formation was progressively inhibited, when mitochondria were resuspended in media containing increasing concentration of KCl (from 0.05 to 0.15  M ). This inhibition was linked to a partial dissipation of the transmembrane electrical potential (ΔΨ) induced by KCl. Conversely, the malate plus glutamate-dependent H₂O₂ formation was not influenced. The succinate-sustained H₂O₂ generation was also unaffected by nigericin (a H⁺/K⁺ exchanger), but completely prevented by valinomycin (a K⁺ ionophore). In addition, cyclosporin A (a K⁺_ATP channel opener) inhibited this H₂O₂ formation, while ATP (an inhibitor of the channel opening) slightly increased it. The inhibitory effect of ATP was strongly stimulated in the presence of atractylate (an inhibitor of the adenine nucleotide translocase), thus suggesting that the receptor for ATP on the K⁺ channel faces the intermembrane space. Finally, the succinate-dependent H₂O₂ formation was partially prevented by phenylarsine oxide (a thiol oxidant).     

Biological oxidation of hydrogen in soils flushed with a mixture of H2, CO2, O2 and N2

Abstract A stainless steel cylinder filled with soil was flushed upstream with a H₂/CO₂/air mixture. The consequence was a strong enrichment of the aerobic, autotrophic hydrogen-oxidising microflora, which reached densities enabling them to oxidize 84.5 ml H₂· dm⁻²· h⁻¹ in the first 25-cm layer. H₂ concentration profiles, hydrogen uptake activity and cell numbers correlated well with each other. Most of the organisms isolated were dinitrogen fixers. Thus, soils containing hydrogen-oxidising bacteria may act as a biological shield between H₂-rich environments and air, and may be utilized as biofilters, e.g., in the waste-processing industry.     

Acetogenesis from H2 and CO2 by methane- and non-methane-producing human colonic bacterial communities

Abstract: The purpose of the study was to define the potential for reductive acetogenesis of colonic microflora from six non-methane- and four methane-excreting human subjects in relation to numbers of the different H₂-utilizing microorganisms. Faecal bacterial suspensions were incubated in the presence of NaH¹³CO₃ and under a gas phase composed of either 100% N₂ (control) or 80% H₂–20% N₂. The effects of a specific methanogenesis inhibitor or of sulfate supplementation were also determined. Quantitative nuclear magnetic resonance showed the presence of both single- and double-labelled acetate in all incubations under hydrogen. H₂/CO₂-acetogenesis appears to be a quantitatively important activity only in the presence of very low numbers of methanogens. Inhibition of methanogenesis induced a large increase in ¹³CO₂ incorporation into acetate in CH₄-producing samples. These results showed that methanogens can efficiently outcompete acetogens in human colonic contents. In contrast, no clear-cut competition for H₂ between acetogenesis and dissimilatory sulfate-reduction could be demonstrated. A slight reduction of the acetogenic activity was only observed at the highest sulfate addition (100 mM).     

Inhibition of Methanosarcina barkeri strain 227 by cadmium

Abstract The effect of cadmium (Cd) on methane formation from methanol and/or H₂–CO₂ by Methanosarcina barkeri was examined in a defined growth medium and in a simplified buffer system containing 50 mM Tes with or without 2 mM dithiothreitol (DTT). No inhibition of methanogenesis by high concentrations of cadmium was observed in growth medium. Similarly, little inhibition of methanogenesis by whole cells in the Tes buffer system was observed in the presence of 430 μM Cd or 370 μM mercury (Hg) with 2 mM DTT. When the concentration of DTT was reduced to 0.4 mM, almost complete inhibition of methanogenesis from H₂–CO₂ and methanol by 600 μM Cd was observed. In the absence of DTT, 150 μM Cd inhibited methanogenesis from H₂–CO₂ completely and from methanol by 97%. Methanogenesis from H₂–CO₂ was more sensitive to Cd than that from methanol.     

HISTAMINE-SENSITIVE ADENYLATE CYCLASE IN HYPOTHALAMUS OF RAT BRAIN: H1 AND H2 RECEPTORS

Abstract— In in vitro experiments on rat hypothalamic homogenates the effects of biogenic amines such as histamine (HA), noradrenaline (NA), dopamine (DA), serotonin (5-HT) and drugs such as isoprenaline (ISP), 2-(2-pyridyl)ethylamine (H₂ stimulant—H_ls), 4-methyl-histamine (H₂ stimulant H_2s), mepyramine (H₁ antagonistp H_la), cimetidine (H₂ antagonist—H_2a) were tested on adenylate cyclase activity. HA possessed a powerful stimulating effect on hypothalamic adenylate cyclase activity, higher than that shown by the other substances.
The stimulating effect of HA was greatest in hypothalamic tissue from male rats, while tissue from females showed only a modest stimulation. H_2s, induced a greater stimulation of adenylate cyclase than H_ls. On the other hand, the H_2a inhibited HA stimulation to a greater extent than the H_la, H_la and H_2a, when used together, completely inhibited the HA stimulation. HA may have a neurotrans-mitter role in the hypothalamus, and in this area there appears to be a mixed population of H₁ and H₂ receptors, with a majority of H₂ receptors.     

Influence of soil O2 and CO2 on root respiration for Agave deserti

Respiration measured as CO₂ efflux was determined at various soil O₂ and CO₂ concentrations for individual, attached roots of a succulent perennial from the Sonoran Desert, Agave deserti Engelm. The respiration rate increased with increasing O₂ concentration up to about 16% O₂ for established roots and 5% O₂ for rain roots (fine branch roots on established roots induced by wetting of the soil) and then remained fairly constant up to 21% O₂. When O₂ was decreased from 21 to 0%, the respiration rates were similar to those obtained with increasing O₂ concentration. The CO₂ concentration in the root zone, which for the shallow-rooted A. deserti in the field was about 1 000 μl l^-1, did not affect root respiration at concentrations up to 2 000 μl l^-1, but higher concentrations reduced it, respiration being abolished at 20 000 μl l^-1 (2%) CO₂ for both established and rain roots. Upon lowering CO₂ to 1 000 μl l^-1 after exposure to concentrations up to 10000 μl l^-1 CO₂, inhibition of respiration was reversible. Uptake of the vital stain neutral red by root cortical cells was reduced to zero, indicating cell death, in about 4 h at 2% CO₂, substantiating the detrimental effects of high soil CO₂ concentrations on roots of A. deserti . This CO₂ response may explain why roots of desert succulents tend to occur in porous, well-aerated soils.     

Symbiotic N2 fixation in a high Alpine grassland: effects of four growing seasons of elevated CO2

1. Increasing carbon dioxide concentration (E: 680 μl CO₂ litre^–1 vs ambient, A: 355 μl CO₂ litre^–1) around late-successional Alpine sedge communities of the Swiss Central Alps (2450 m) for four growing seasons (1992–1995) had no detectable effect on symbiotic N₂ fixation in Trifolium alpinum —the sole N₂-fixing plant species in these communities (74 ± 30 mg N m^–2 year^–1, A and E plots pooled).
2. This result is based on data collected in the fourth growing season showing that elevated CO₂ had no effect on Trifolium above-ground biomass (4·4 ± 1·7 g m^–2, A and E plots pooled, n = 24) or N content per unit land area (124 ± 51 mg N m^–2, A and E pooled), or on the percentage of N Trifolium derived from the atmosphere through symbiotic N₂ fixation (%Ndfa: 61·0 ± 4·1 across A and E plots) estimated using the ¹⁵N dilution method.
3. Thus, it appears that N inputs to this ecosystem via symbiotic N₂ fixation will not be dramatically affected in the foreseeable future even as atmospheric CO₂ continues to rise.     

The oxidative stress response in Enterococcus faecalis: relationship between H2O2 tolerance and H2O2 stress proteins

The hydrogen peroxide (H₂O₂) stress response in Enterococcus faecalis ATCC19433 was investigated. A 2·4 mmol l⁻¹ H₂O₂ pretreatment conferred protection against a lethal concentration (45 mmol l⁻¹) of this agent. The relatively high concentrations of H₂O₂ used for adaptation and challenge treatments in Ent. faecalis emphasised the strong resistance towards oxidative stress in this species. Various stresses (NaCl, heat, ethanol, acidity and alkalinity) induced weak or strong H₂O₂ cross-protection. This paper describes the involvement of protein synthesis in the active response to lethal dose of H₂O₂, in addition to the impressive enhancement of synthesis of five H₂O₂ stress proteins. Combined results suggest that these proteins might play an important role in the H₂O₂ tolerance response.     

Carbon and water fluxes in a calcareous grassland under elevated CO2

1. As part of a long-term study of the effects of elevated CO₂ on biodiversity and ecosystem function in a calcareous grassland, we measured ecosystem carbon dioxide and water-vapour fluxes over 24-h periods during the 1994 and 1995 growing seasons. Data were used to derive CO₂ and H₂O gas-exchange response functions to quantum flux density (QFD).
2. The relative increase in net ecosystem CO₂ flux (NEC) owing to CO₂ enrichment increased as QFD rose. Daytime NEC at high QFD under elevated CO₂ increased by 25% to 60%, with the greatest increases in the spring and after mowing in June when above-ground biomass was lowest. There was much less stimulation of NEC in early June and again in October when the canopy was fully developed. Night-time NEC was not significantly altered under elevated CO₂.
3. Short-term reversal of CO₂ concentrations between treatments after two seasons of CO₂ exposure provided evidence for a 50% downward adjustment of NEC expressed per unit above-ground plant dry weight. However, when expressed on a land area basis, this difference disappeared because of a c. 20% increase in above-ground biomass under elevated CO₂.
4. Ecosystem evapotranspiration (ET) was not significantly altered by elevated CO₂ when averaged over all measurement dates and positions. However, ET was reduced 3–18% at high QFD in plots at the top of the slope at our study site. In summary, CO₂ enrichment resulted in a large stimulation of ecosystem CO₂ capture, especially during periods of a large demand of carbon in relationship to its supply, and resulted in a relatively small and variable effect on ecosystem water consumption.     

Relationship between C2H2 reduction, H2 evolution and 15N2 fixation in root nodules of pea (Pisum sativum)

The quantitative relationship between C₂H₂ reduction, H₂ evolution and ¹⁵N₂ fixation was investigated in excised root nodules from pea plants ( Pisum sativum L. cv. Bodil) grown under controlled conditions. The C₂H₂/N₂ conversion factor varied from 3.31 to 5.12 between the 32nd and the 67th day after planting. After correction for H₂ evolution in air, the factor (C₂H₂-H₂)/N₂ decreased to values near the theoretical value 3, or in one case to a value significantly ( P < 0.05) below 3. The proportion of the total electron flow through nitrogenase, which is not wasted in H₂ production but used for N₂ reduction, is often stated as the relative efficiency (1-H₂/C₂H₂). This factor varied significantly ( P < 0.05) during the growth period. The actual allocation of electrons to H₂ and N₂, expressed as the H₂/N₂ ratio, was independent of plant age, however. This discrepancy and the observation that the (C₂H₂-H₂)/N₂ conversion factor tended to be lower than 3, suggests that the C₂H₂reduction assay underestimates the total electron flow through nitrogenase.     

Sodium bioenergetics in methanogens and acetogens

Abstract Recent investigations with Methanosarcina barkeri elucidated the role of sodium ions in the energy metabolism of methanogenic bacteria and provided evidence for a novel mechanism of energy transduction with Na⁺ as the coupling ion. During methanogenesis from methanol, an eletrochemical sodium gradient generated by a Na⁺/H⁺ antiporter is used as the driving force for the thermodynamically unfavourable oxidation of methanol to the formal redox level of formaldehyde. During methanogenesis from H₂+ CO₂, the reverse reaction, the reduction of formaldehyde to the level of methanol, is accompanied by a primary, electron transport-driven sodium extrusion. Acetogenesis from H₂+ CO₂ as carried out by Acetobacterium woodii is a sodium-dependent process and is accompanied by the generation of a transmembrane sodium gradient with the reduction of formaldehyde to the level of methanol as the sodium-dependent step.     

Effects of raised CO2 on potential CH4 production and oxidation in, and CH4 emission from, a boreal mire

1 In a glasshouse experiment we studied the effect of raised CO₂ concentration (720 p.p.m.) on CH₄ emission at natural boreal peat temperatures using intact cores of boreal peat with living vascular plants and Sphagnum mosses. After the end of the growing season half of the cores were kept unnaturally warm (17–20 °C). The potential for CH₄ production and oxidation was measured at the end of the emission experiment.
2 The vascular cores ('Sedge') consisted of a moss layer with sedges, and the moss cores (' Sphagnum ') of Sphagnum mosses (some sedge seedlings were removed by cutting). Methane efflux was 6–12 times higher from the Sedge cores than from the Sphagnum cores. The release of CH ₄ from Sedge cores increased with increasing temperature of the peat and decreased with decreasing temperature. Methane efflux from Sphagnum cores was quite stable independent of the peat temperatures.
3 In both Sedge and Sphagnum samples, CO₂ treatment doubled the potential CH₄ production but had no effect on the potential CH₄ oxidation. A raised concentration of CO₂ increased CH₄ efflux weakly and only at the highest peat temperatures (17–20 °C).
4 The results suggest that in cool regions, such as boreal wetlands, temperature would restrict decomposition of the extra substrates probably derived from enhanced primary production of mire vegetation under raised CO₂ concentrations, and would thus retard any consequent increase in CH₄ emission.     

Ca2+/Calmodulin-Mediated Regulation of Agonist-Induced Sequestration of Gq Protein-Coupled Histamine H1 Receptors in Human U373 MG Astrocytoma Cells

Abstract: We investigated the regulation by intracellular Ca²⁺ of agonist-induced sequestration of G_q protein-coupled histamine H₁ receptors in human U373 MG astrocytoma cells. Histamine-induced sequestration of H₁ receptors from the cell surface membrane was detected as the loss of [³H]mepyramine binding sites on intact cells accessible to the hydrophilic H₁-receptor antagonist pirdonium. The changes in the pirdonium-sensitive binding of [³H]mepyramine were mirrored by changes in the subcellular distribution of H₁ receptors detected by sucrose density gradient centrifugation. The histamine-induced sequestration of H₁ receptors did not occur in hypertonic medium, in which clathrin-mediated endocytosis is known to be inhibited, but was significantly accelerated in the absence of extracellular Ca²⁺ or in the presence of the calmodulin antagonists W-7 and calmidazolium. Inhibitors of protein kinase C (H-7 and GF109203X), Ca²⁺/calmodulin-dependent protein kinase II (KN-62), or protein phosphatase 2B (FK506) did not alter the time course of H₁-receptor sequestration. These results provide the first evidence that agonist-induced, clathrin-mediated sequestration of G_q protein-coupled receptors is transiently inhibited by Ca²⁺/calmodulin, with the result that receptors remain on the cell surface membrane during the early stage of agonist stimulation.     

Elevated concentrations of atmospheric CO2 protect against and compensate for O3 damage to photosynthetic tissues of field-grown wheat

The effects of elevated concentrations of atmospheric carbon dioxide and ozone on diurnal patterns of photosynthesis have been investigated in field-grown spring wheat ( Triticum aestivum ). Plants cultivated under realistic agronomic conditions, in open-top chambers, were exposed from emergence to harvest to reciprocal combinations of two carbon dioxide and two ozone treatments: [CO₂] at ambient (380 μmol mol⁻¹, seasonal mean) or elevated (692 μmol mol⁻¹) levels, [O₃] at ambient (27 nmol mol⁻¹, 7 hr seasonal mean) or elevated (61 nmol mol⁻¹) levels. After anthesis, diurnal measurements were made of flag-leaf gas-exchange and in vitro Rubisco activity and content. Elevated [CO₂] resulted in an increase in photoassimilation rate and a loss of excess Rubisco activity. Elevated [O₃] caused a loss of Rubisco and a decline in photoassimilation rate late in flag-leaf development. Elevated [CO₂] ameliorated O₃ damage. The mechanisms of amelioration included a protective stomatal restriction of O₃ flux to the mesophyll, and a compensatory effect of increased substrate on photoassimilation and photosynthetic control. However, the degree of protection and compensation appeared to be affected by the natural seasonal and diurnal variations in light, temperature and water status.     

Soil CO2 efflux in a boreal pine forest under atmospheric CO2 enrichment and air warming

The response of forest soil CO₂ efflux to the elevation of two climatic factors, the atmospheric concentration of CO₂ (↑CO₂ of 700 μmol mol⁻¹) and air temperature (↑ T with average annual increase of 5°C), and their combination (↑CO₂+↑ T ) was investigated in a 4-year, full-factorial field experiment consisting of closed chambers built around 20-year-old Scots pines ( Pinus sylvestris L.) in the boreal zone of Finland. Mean soil CO₂ efflux in May–October increased with elevated CO₂ by 23–37%, with elevated temperature by 27–43%, and with the combined treatment by 35–59%. Temperature elevation was a significant factor in the combined 4-year efflux data, whereas the effect of elevated CO₂ was not as evident. Elevated temperature had the most pronounced impact early and late in the season, while the influence of elevated CO₂ alone was especially notable late in the season. Needle area was found to be a significant predictor of soil CO₂ efflux, particularly in August, a month of high root growth, thus supporting the assumption of a close link between whole-tree physiology and soil CO₂ emissions. The decrease in the temperature sensitivity of soil CO₂ efflux observed in the elevated temperature treatments in the second year nevertheless suggests the existence of soil response mechanisms that may be independent of the assimilating component of the forest ecosystem. In conclusion, elevated atmospheric CO₂ and air temperature consistently increased forest soil CO₂ efflux over the 4-year period, their combined effect being additive, with no apparent interaction.     

Interaction of elevated CO2 and O3 on growth, photosynthesis and respiration of three perennial species grown in low and high nitrogen

Seedlings of three species native to central North America, a C₃ tree, Populus tremuloides Michx., a C₃ grass, Agropyron smithii Rybd., and a C₄ grass, Bouteloua curtipendula Michx., were grown in all eight combinations of two levels each of CO₂, O₃ and nitrogen (N) for 58 days in a controlled environment. Treatment levels consisted of 360 or 674 μmol mol^-1 CO₂, 3 or 92 nmol mol^-1 O₃, and 0.5 or 6.0 m M N. In situ photosynthesis and relative growth rate (RGR) and its determinants were obtained at each of three sequential harvests, and leaf dark respiration was measured at the second and third harvests. In all three species, plants grown in high N had significantly greater whole-plant mass, RGR and photosynthesis than plants grown in low N. Within a N treatment, elevated CO₂ did not significantly enhance any of these parameters nor did it affect leaf respiration. However, plants of all three species grown in elevated CO₂ had lower stomatal conductance compared to ambient CO₂-exposed plants. Seedlings of P. tremuloides (in both N treatments) and B. curtipendula (in high N) had significant ozone-induced reductions in whole-plant mass and RGR in ambient but not under elevated CO_2. This negative O₃ impact on RGR in ambient CO₂ was related to increased leaf dark respiration, decreased photosynthesis and/or decreased leaf area ratio, none of which were noted in high O₃ treatments in the elevated CO₂ environment. In contrast, A. smithii was marginally negatively affected by high O_3.     

Hydrogen Peroxide Induces a Long-Lasting Inhibition of the Ca2+-Dependent Glutamate Release in Cerebrocortical Synaptosomes Without Interfering with Cytosolic Ca2+

Abstract: We studied the action of H₂O₂ on the exocytosis of glutamate by cerebrocortical synaptosomes. The treatment of synaptosomes with H₂O₂ (50–150 µ M ) for a few minutes results in a long-lasting depression of the Ca²⁺-dependent exocytosis of glutamate, induced by KCl or by the K⁺-channel inhibitor 4-aminopyridine. The energy state of synaptosomes, as judged by the level of phosphocreatine and the ATP/ADP ratio, was not affected by H₂O₂, although a transient decrease was observed after the treatment. H₂O₂ did not promote peroxidation, as judged by the formation of malondialdehyde. In indo-1-loaded synaptosomes, the treatment with H₂O₂ did not modify significantly the KCl-induced increase of [Ca²⁺]_i. H₂O₂ inhibited exocytosis also when the latter was induced by increasing [Ca²⁺]_i with the Ca²⁺ ionophore ionomycin. The effects of H₂O₂ were unchanged in the presence of superoxide dismutase and the presence of the Fe³⁺ chelator deferoxamine. These results appear to indicate that H₂O₂, apparently without damaging the synaptosomes, induces a long-lasting inhibition of the exocytosis of glutamate by acting directly on the exocytotic process.